Conventional seismic data processing method uses hyperbolic equation to describe time-distance formula of reflection wave, error of this equation increases with the increase of heterogeneity, anisotropy and spread length.
英
美
- 常規地震資料處理方法是利用雙曲線(xiàn)方程來(lái)描述反射波時(shí)距曲線(xiàn)規律，此方程隨著(zhù)地層非均質(zhì)性、各向異性和排列長(cháng)度的增加，其誤差變大。
